Richard H. Tice, and others
1957, Open-File Report 57-111
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Publication Extents
Not all publications have extents, not all extents are completely accurateLeonard Shapiro, Walter Wallace Brannock
1957, Open-File Report 57-99
The method is an adaptation of a procedure described by Betz and Noll1 in 1950. Calcium and magnesium are determined by visual titration using Versene (disodium ethylenediamine tetraacetate) with Murexide (ammonium purpurate) as the indicator for calcium and Eriochrome Black T as the indicator for magnesium....
Erwin J. Lyons
1957, Open-File Report 57-66
Cane Branch and Helton Branch in McCreary County, Kentucky, are about 1.4 miles apart (fig. 1). Can Branch, which is about 2.1 miles long, emptied into Hughes Fork of Beaver Creek. Its watershed area of about 1.5 square miles lies largely in the Wiborf 7 1/2-minute quadrangle (SW/4 Cumberland Falls...
M. R. Klepper, R. A. Weeks, E. T. Ruppel
1957, Professional Paper 292
The geology of an area of about 270 square miles in the southern Elkhorn Mountains, west of Townsend in west-central Montana, is described. The mountains in the southern part of the area comprise northward-trending alternating ridges and valleys underlain principally by folded sedimentary rocks. They merge northward into the higher...
Kathleen McQueen, R.G. Ray
1957, Trace Elements Memorandum 1022
No abstract available...
Louis D. Carswell, Edward S. Davidson, Glen A. Miller
1957, Trace Elements Memorandum 1061
No abstract available...
N. P. Cuppels, F.R. Conwell
1957, Trace Elements Memorandum 1049
No abstract...
D.A. Brobst
1957, Trace Elements Memorandum 1047
No abstract available...
J. S. Pomeroy
1957, Trace Elements Memorandum 1017
No abstract available...
R. W. Schnabel, L.J. Charlesworth Jr.
1957, Trace Elements Memorandum 1058
No abstract available...
J. S. Pomeroy
1957, Trace Elements Memorandum 1018
No abstract available...
Kathleen McQueen
1957, Trace Elements Memorandum 1015
No abstract available...
Edwin V. Post, Donald W. Lane
1957, Trace Elements Memorandum 1053
No abstract available...
R. W. Schnabel
1957, Trace Elements Memorandum 1059
No abstract available...
Edwin V. Post
1957, Trace Elements Memorandum 1055
No abstract available...
R. W. Schnabel, L.J. Charlesworth Jr.
1957, Trace Elements Memorandum 1057
No abstract available...
Kathleen McQueen
1957, Trace Elements Memorandum 1021
No abstract available...
Edwin V. Post
1957, Trace Elements Memorandum 1054
No abstract available...
O.J. Larimer
1957, Iowa Highway Research Board Bulletin 7
The drainage area of a stream at a specified location ordinarily may be defined as that area, measured in a horizontal plane, which is enclosed by a topographic divide such that direct surface runoff from precipitation would drain by gravity into the river basin above the specified point. One of the...
Edwin V. Post, Norman P. Cupples
1957, Trace Elements Memorandum 1052
No abstract available...
W.P. Hemphill
1957, Trace Elements Memorandum 1020
No abstract available...
Glen A. Miller, Robert A. Cadigan
1957, Trace Elements Memorandum 1062
No abstract available...
R.G. Petersen, D. A. Phoenix
1957, Trace Elements Memorandum 1027
No abstract available...
W.P. Hemphill
1957, Trace Elements Memorandum 1019
No abstract available...
C. A. Kaye
1957, GSA Bulletin (68) 103-118
Two major structural and stratigraphic rock units occur in Puerto Rico: the older complex, ranging in known age from Late Cretaceous to late Paleocene or early Eocene and the middle Tertiary sequence, ranging from late Oligocene possibly to late Miocene. The former rocks are eugeosynclinal in character and are very...